[unav_all] AGU Special Sessopm
Timothy H.Dixon
tdixon at rsmas.miami.edu
Thu Aug 16 09:59:54 MDT 2007
Dear Colleagues,
We would like to call your attention to Session G06 "Geodesy and
Geophysics of Coastal Subsidence, Regional Sea Level Rise, and
Consequences" at fall AGU.
Coastal subsidence and regional sea level rise combine to form an
important interdisciplinary scientific problem, with critical
implications as people and property are increasingly at risk.
The session description is below. Abstracts are due Sept. 6th.
Thank you!!! and apologies for multiple posts.....
Ron Blom, Tim Dixon, Bert Vermeersen
____________
Session description.
Convener:
Ronald G. Blom
Jet Propulsion Laboratory
M/S 300-233
4800 Oak Grove Drive
Pasadena, CA, USA 91109
818-354-4681
ronald.blom at jpl.nasa.gov
Timothy H. Dixon
University of Miami
RSMAS-MGG, N374
4600 Rickenbacker Cswy.
Miami, FL, USA 33149
305-421-4660
tdixon at rsmas.miami.edu
Bert Vermeersen
TU Delft
Kluyverweg 1
Delft, NLD 2629HS
+31 (0)15 27 88272
L.L.A.Vermeersen at tudelft.nl
Coastal subsidence and regional sea level rise combine to form an
important interdisciplinary scientific problem, with critical
implications as people and property are increasingly at risk. The
geophysical processes involved are incompletely understood, and
specific contributions of various components of different spatial and
temporal scales are poorly known. Significantly, regional sea level
change can differ considerably from global-averaged values; in fact, in
many places there is actually a sea-level drop (e.g. formerly glaciated
areas). Meanwhile, areas such as the Mississippi delta show rapid
relative sea level rise due to subsidence caused by multiple factors.
The simple notion of a uniform redistribution of present-day meltwater
over the world's oceans is incorrect due to the self-gravitation effect
("fingerprinting"). Local or regional authorities need to know what
sea-level will be at their location, and this will likely differ
substantially from this global average. In terms of sea-level change,
any measurements of long-term sea-level rise are complicated by
complex, non-secular signals which occur on seasonal, interannual and
decadal time scales and vary by region. These non-secular variations
are potentially important in accounting for observed discrepancies
between historic tide-gauge data and data from recent altimeter
missions such as TOPEX/Poseidon and Jason-1, and make it difficult to
assess accelerations in sea-level rise. Many of these variations have
oceanographic origins and are interesting in their own right as a key
to understanding the global water budget. Crustal deformation, from
sources such as sediment loading, post-seismic deformation after large
earthquakes, and unloading as ice sheets melt, will also be evident in
the tide-gauge record, and coastal subsidence will also cause
non-secular signals for certain regions. Various space based data sets
(GPS, InSAR, GRACE, LandSAT, ASTER, etc.), state of the art geodesy,
and new geophysical modeling capabilities, all can be used to improve
understanding of the underlying physics. Accurate measurement and
prediction is vital for dealing with changing sea levels. In this
session we seek to bring together scientists from diverse disciplines
to discuss the current state of understanding of secular, non-secular,
and regional changes in sea level, and the future impacts to changing
coastlines. Focus will be given to studies that separate signals of a
particular origin, either geodetic or oceanographic, seasonal or
longer-period, from measurements of sea level and/or coastal
subsidence. Modeling studies or synthesis efforts involving the
combination of models and data are also emphasized. Case studies of
specific regions are of particular interest. Studies that include or
focus on ways this information has been used by planners or
policymakers are welcome.
Tim Dixon
Professor, University of Miami
RSMAS-MGG
4600 Rickenbacker Cswy
Miami, FL 33149
305 421 4660 (office)
305 421 4928 (Lab)
305 323 1820 (cell)
305 421 4632 (fax)
email: tdixon at rsmas.miami.edu
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